Journal of Global Change Data & Discovery2017.1(3):324-330

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Citation:Liu, C., Shi, R. X.Boundary Data for Asia Tropical Humid & Semi-humid Eco-region[J]. Journal of Global Change Data & Discovery,2017.1(3):324-330 .DOI: 10.3974/geodp.2017.03.11 .

Boundary Data for Asia Tropical Humid & Semi- humid Eco-region

Liu, C.  Shi, R. X.*

Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China

 

 

Abstract: The Asia tropical humid and semi-humid eco-region is located within the region of the tropical rain forest and Asia monsoon forest; it is the region with the most islands of the world. The total area of the region is 680.93×104 km2. It has 9,600 islands with a total area of 177.94×104 km2, which is 26.13% of the total area of this region. This study identifies the eco-regions by using ecosystem indicators. Based on data from NASA’s Earth Observation System and the eco-system regionalization model, we locate the boundaries of the eco-region. The indicators are as follows: (1) 16 °C is the average temperature of the coldest month for dividing tropical from sub-tropical regions; (2) 7° is the slope of the landform; and (3) 400 mm annual rainfall divides semi-humid from humid regions. The boundary of the Asia tropical humid and semi-humid eco-region extends from south Taiwan, south of the Leizhou Peninsula of Guangdong Province, to Guangxi and Yunnan Provinces to the west of China linking with the roof of the world eco-region, then to the west of India, Pakistan, then to the east of Karachi and to the nearby coastline. The Asia tropical humid and semi-humid eco-region includes a series of islands, including the Maldives islands, the British islands in the Indian Ocean, Sri Lanka and its surrounding islands, the Indonesia islands to Bali Island, Kalimantan Island, and the Philippines to Taiwan. The region covers countries including China, India, Pakistan, Sri Lanka, Myanmar, Laos, Vietnam, Malaysia, Singapore, Thailand, Cambodia, Brunei, the Philippines, Indonesia, etc. The data are archived in both .kmz and .shp formats with a compressed data size of 76.5 MB.

Keywords: Asia; tropic; humid; semi-humid; eco-region; regionalization

1 Introduction

The Asia tropical humid and semi-humid eco-region is located at the region of the tropical rain forest and Asia monsoon forest; it is the region of the world with the most islands. Fourteen countries partake in this region, including China, India, Pakistan, Sri Lanka, Myanmar, Laos, Vietnam, Malaysia, Singapore, Thailand, Cambodia, Brunei, the Philippines, and Indonesia. The total area of the region is 680.93×104 km2. It contains 9,600 islands with a total area of 177.94×104 km2, which is 26.13% of total area of this region. The biggest islands include Kalimantan Island with an area of 73.20×104 km2 and Hainan Island with an area of 3.40×104 km2. The total coastline measures 14.11×104 km, which is 86.61% of the total outlines of the region. The Asia tropical humid and semi-humid eco-region is the only tropical forest region in Asia; it is the region with the most biodiversity in Asia. Based on the eco-regionalization method[1] and an analysis of remote-sensing data, we report herein the boundary data for this region.

2 Metadata of Dataset

The metadata summary for Boundary data of Asia tropical humid & semi-humid eco-region (ATHSBND)[2] are listed in Table 1.

Table 1  Summary of ATHSBND data

Item

Discription

Title of Dataset

Boundary data of Asia tropical humid & semi-humid eco-region

Short Name of Dataset

ATHSBND

Authors

Liu, C. L-3684-2016, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, lchuang@igsnrr.ac.cn

Shi, R. X. L-4389-2016, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, shirx@igsnrr.ac.cn

Region

Geolocation: 34º32′47.33″N-12º12′32.17″S, 68º23′48.07″E-126º36′19.05″E, including China, India, Pakistan, Sri Lanka, Myanmar, Laos, Vietnam, Malaysia, Singapore, Thailand, Cambodia, Brunei, Philippines and Indonesia

Year

2014

Spatial resolution

30 m

Data formats

.shp, .kmz, .rar

Data files

The dataset include two data files, one is in compressed .shp format (ATHSBND.rar, 57.2 MBand other one is .kmz data format (ATHSBND.kmz, 19.3 MB)

Data size

76.5 MBcompressed

Foundation

Chinese Academy of Sciences (INF0-115-C01-SDB3-02); Ministry of Science and Technology of P. R. China (2017YFA0604701)

Publisher

Global Change Research Data Publishing & Repository, http://www.geodoi.ac.cn

Address

No. 11A, Datun Road, Chaoyang District, Beijing 100101, China

Data sharing policy

Data from the Global Change Research Data Publishing & Repository includes metadata, datasets (data products), and publications (in this case, in the Journal of Global Change Data & Discovery). Data sharing policy includes: (1) Data are openly available and can be free down-loaded via the Internet; (2) End users are encouraged to use Data subject to citation; (3) Users, who are by definition also value-added service providers, are welcome to redistribute Data subject to written permission from the GCdataPR Editorial Office and the issuance of a Data redistribution license; and (4) If Data are used to compile new datasets, the ‘ten percent principal’ should be followed such that Data records utilized should not surpass 10% of the new dataset contents, while sources should be clearly noted in suitable places in the new dataset[3]

3 Methodology of Dataset Development

Based on the method for eco-regionalization, the ATHSBND are developed by using the following indicators: (1) 16 °C is the average temperature of the coldest month for dividing tropical from sub-tropical regions; (2) the slope of landform is 7°; and (3) 400 mm annual rainfall and vegetation divides the semi-humid from the humid regions. Figure 1 shows the procedure for developing the dataset.

The following data sources were used to develop the dataset: the

average temperature of the coldest month and the annual rainfall data are from WorldClim—Global Climate Data[4]; the Advanced Spaceborne Thermal Emission and Reflection Radiometer Global Digital Elevation Model comes from the Distributed Active Archive Center of the US Geological Survey[5], the MODIS Normalized Difference Vegetation Index (NDVI) comes from the University of Maryland, USA[6], the coastline data come from the US National Geophysical Data Center[7], and the global ecosystem regions data come from the Food and Agriculture Organization (FAO) of the United Nations[8].

Figure 1  Flowchart for developing ATHSBND

3.1 Boundaries between Asia Tropical Humid & Semi-humid Region and East Asia Summer Monsoon Eco-region

The major difference between the Asia tropical humid and semi-humid eco-region and east Asia summer monsoon eco-region is the winter temperature. According to the Koppen Climate Classification[9], FAO[8] eco-regionalization, and scientists from China and Vietnam[10–25], the indicator dividing the Asia Sub-Tropic and Temperature Masson eco-region in terms of climate, ecosystems, agriculture, and vegetation is the average temperature in January, which is the coldest month. The only difference between the two regions is that the Koppen Climate Classification uses 18 °C as the indicator, whereas most Chinese researchers use 16 °C as the indicator[18–22]. Tang[10], Yu[16], and the team from the Agriculture Resources and Regions of China[24] use 15 °C as the indicator.

The present study uses an average temperature of 16 °C in January as one of the indicators. The remaining indicators are determined based on the land slope classification (land slope must be less than 7° in general), the China climate regionalization[18], the Vietnam Agricultural climate resources and regionalization[25], coastline data from the US National Geophysical Data Center,[7] and Google Earth images. The boundaries between the Asia sub-tropic and the east Asia summer monsoon eco-region include three major parts:

(1) Line dividing Yunnan, China from northern Vietnam. This boundary is 5,613.92 km long, with the northern most part at 24°15′27″ N, 101°27′47″ E. The mountains running from the northwest to southeast facilitate the passage of warm wet air to the northernmost regions (Figure 2).

Figure 2  Comparison of ATHSBND boundary in Yunan, China and northern Vietnam with the 16 °C

average-January-temperature line

Figure 3  Comparison of ATHSBND boundary of

Leizhou Peninsula with 16 °C average-

January-temperature line

Figure 4  Comparison of ATHSBND boundary near Taiwan with 16 °C average-January-temperature line

(2) Boundary line south of Leizhou Peninsula. The boundary follows the foothills and plains from northern Maoming City and Huazhou City. This line is about 30 km north of the line for 16 °C average temperature in January. The northernmost place is Gaozhou City of Guangdong Province at 21°55′17″N (Figure 3).

(3) Boundary line south of Taiwan. This dividing line runs along the southern coastline of Taiwan at elevations less than 500 m above sea level. The most northern part is Banxia county of Hualian City at 24°10′51″N. On the western coastline, it reaches the Daxi river between Zhanghua City and Taizhong City at 24°11′51″N (Figure 4).

3.2 Boundary between Asia Tropical Humid & Semi-humid Region and Roof of the World Region

The boundary between the Asia tropic and the Roof of the World eco-regions was described by Liu[26,27]. The indicators include elevation (4,000 m), land slope (), and vertical mountain ecosystems. The boundary is 6,927.37 km long (Figure 5).

3.3 Boundary between Asia Tropical Humid & Semi-humid Eco-region and West Asia & North Africa Tropical and Sub-tropical Dry Land Eco-region

The indicators for dividing these eco- regions include annual rainfall and

vegetation[28–31].

The index of the annual rainfall is 400 mm and the NDVI is 0.55 (Figure 6). The boundary is 51,84.21 km long.

4 Data

Figure 7 shows the ATHSBND. The total area of the region, including con tinent and islands, is 680.93×104 km2, of which 177.94×104 km2 come from the 9,600 islands. Thus, the islands account for 26.13% of the total area of this region.

Figure 5  Boundary between Asia tropical humid and semi-humid region and Roof of the World region

Figure 6  Comparison of 400 mm annual rainfall with NDVI for dividing Asia tropical humid and semi-humid region from ATHSBND region

Figure 7  Map of Asia tropical humid and semi-humid eco-region

The ATHSBND dataset consists of two data files:

(1) The compressed boundary (line) and area (polygon) data in .shp format. The file name is ATHSBND.rar, and the data size is 57.2 MB.

(2) The ATHSBND dataset is the boundary (line) data in .kmz format. The file name is ATHSBND.kmz and the data size is 19.3 MB.

5 Discussion

The following issues are of interest for discussion:

(1) Where is the northernmost part of the ATHSBND region?

The ATHSBND indicate that the northernmost part of the ATHSBND region is close to the boundary between the tropical and sub-tropical zones, as indicated by Tang (1959, 1964)[10,13], Zeng (1966, 1980)[14,19], Yu (1981)[16], and Xu (1964, 1982)[21,22]. It means the boundary of the ATHSBND crossing China. If so, China consists of four eco-regions (the eastern monsoon eco-region, the northwestern dry land eco-region, the Tibetan eco-region, and the southern tropic islands eco-region)[32] instead of three eco-regions (eastern monsoon eco-region, northwestern dry land eco-region, and Tibetan eco-region).

(2) Coastline and outline of continents and islands

Normally, coastline is where land meets sea or ocean. However, the sea rises and falls because of tides, making it very hard to get coastline data for the entire region from remote-sensing images in a single acquisition. Thus, we use herein the outline of continents and islands based on Google Earth images (Figure 8). Another issue is the boundary between sea and rivers, especially in river deltas. The solution used herein is to determine the level reached by the sea based on the method of comprehensive consideration.

Figure 8  Map of coastline data matches with

Google Earth images

(3) Administration boundary and boundary of geo-ecosystem region

The Asia tropical humid and semi-

humid eco-region is part of the global ecosystem, so the aim of global regionalization is not only to identify differences between regions, but also to support global and regional governance of sustainable development. This goal requires the comprehensive consideration of both ecosystems and administrative boundaries. The International Centre for Integrated Mountain Development uses the administrative boundaries of the Hindu Kush Himalaya region.

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